干旱气候变化与可持续发展

古海洋学

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  • 同济大学海洋地质系  上海  200092
汪品先

收稿日期: 1993-04-14

  网络出版日期: 1994-07-01

本文引用格式

汪品先 . 古海洋学[J]. 地球科学进展, 1994 , 9(4) : 94 -96 . DOI: 10.11867/j.issn.1001-8166.1994.04.0094

参考文献

[1] 许靖华.古海洋学的历史与趋势.海洋学报,1984, 6(6) :830-842.
[2] Shackleton N J and Kennett J P. Paleotemperature history of the Cenozoic and the initiation of Antarctic glaciation: oxygen and carbon isotopic analyses in DSDP sites 277, 279, 281. Initial Reports of the DSDP 29. 1975, 743-755.
[3] 同济大学海洋地质系.古海洋学概论.同济大学出版社,1989. 315.
[4] CLIMAP Project Members. The surface of the ice age Earth. Science,1976, 191:1131-1137.
[5] Imbrie J et al. On the structure and origin of major glaciation cycles. 1. Linear responces to Milankovitch forcing. Paleoceanography, 1992, 7(6):701-738.

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